Topics > Geography > Rivers > River Glen > College Burn
College Burn
College Burn is river in Northumberland which is a tributary of the River Glen. College Burn arises on the slopes of The Cheviot (hill) and flows aproximately 17km in a roughly northerly direction before it's conflence with Bowmont Water to form the River Glen, near Westnewton. Hethpool Linn (waterfall) is a notable feature of the burn.
 
from Geograph (geograph)
College Burn east of footbridge near Hethpool Linn
Pinned by Simon Cotterill
 
from https://environment.data.gov.…
    College Burn from Source to Lambden Burn
    
    Added by
Simon Cotterill
 
    
  Co-Curate Page
    Hethpool
    - Overview Map Street View HEATHPOOL, a township, in the parish of KirkNewton, union, and W. division of the ward, of Glendale, N. division of Northumberland; containing 51 inhabitants, and comprising …
         
    
  Co-Curate Page
    Westnewton, Northumberland
    - Overview Map Street View NEWTON, WEST, a township, in the parish of Kirk-Newton, union of Glendale, W. division of Glendale ward, N. division of Northumberland, 5¾ miles (W. by N.) …
        
 
from Geograph (geograph)
College Burn east of footbridge near Hethpool Linn
Pinned by Simon Cotterill
 
from https://environment.data.gov.…
    College Burn from Source to Lambden Burn
    
    Added by
Simon Cotterill
 
    
  Co-Curate Page
    Hethpool
    - Overview Map Street View HEATHPOOL, a township, in the parish of KirkNewton, union, and W. division of the ward, of Glendale, N. division of Northumberland; containing 51 inhabitants, and comprising …
            
         
    
 
                         
 
 
 
 
 
 
 
 
 
 
 
 
                                 
                                 
                                 
                                        
                                     
                                        
                                     
                                        
                                     
                                        
                                     
                                        
                                     
                                        
                                    